Why the Moon Is a Copy of Earth? The Fluidity Clue ✎ express

Original: "Giant impact between high-viscosity Theia and low-viscosity proto-Earth: Origin of lunar isotopic crisis"
· Wenshuai Liu
arXiv:2606.20398 · 2026-06-18 · arXiv non-exclusive · independent analysis · 1 min
The collision of solid Theia with a liquid Earth explains why the Moon is so similar to our planet.

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Young Earth was a boiling sphere of liquid rock, while Theia, which crashed into it, had had time to cool and solidify.

It’s like dropping a chunk of cold butter into a pot of soup: the soup splashes out, but the butter barely moves.

Similarly, Earth’s interior spewed into space, forming a cloud of cosmic dust and debris. From this, the Moon gradually coalesced. This hypothesis complements the standard model of the giant impact.

Analysis of lunar soil using light analysis (pioneered by Joseph von Fraunhofer) revealed that the atomic composition of the Moon and Earth is nearly identical. Decades of mystery were solved: due to the difference in fluidity, it was mostly Earth material that escaped into space. The most unexpected outcome: the Moon rocks brought back by the Apollo missions are frozen splashes of our planet. Holding them, you’re touching a shard of ancient Earth.

That same impact likely tilted Earth’s axis, giving us the seasons. So we have spring and autumn to thank that ancient catastrophe for.

Scientists
Isaac NewtonJohn MichellRobert HookeJames JeansGalileo GalileiJohn Henry Poynting
Concepts
lunar formation giant impact asteroid impact magma ocean titan oxidation mantle planetesimal formation Moon planetary embryo planet super earth solar system asteroid belt rocky planet planetary accretion chemistry tidal heating protoplanetary disk hydrogen atmosphere gap mars